The Earth’s atmosphere and the Earth itself behave exactly like the plates of a capacitor. This type of system could revolutionize the current energy system, finally achieving non-polluting energy independence from traditional electricity sources—coal, oil, diesel, and nuclear.
The Electro-Radiant Event is produced when a high-voltage direct current is discharged through a spark gap and suddenly interrupted before any current reversal can occur, keeping this so-called “cold” energy available in large quantities. This effect is greatly enhanced when the direct current source is a charged capacitor, which in our specific case could be represented by the entire planet. The Electro-Radiant Event abandons the cables and other components of current-design circuits…

The Electro-Radiant Event produces a spatially distributed voltage that can be thousands of times higher than the voltage of the initial spark discharge. This voltage propagates instantaneously as a longitudinal, electrostatic “light-like ray.” This beam behaves similarly to an incompressible gas under pressure, with luminous effects seen in vacuum globes. The Earth’s crust is an excellent conductor of electrical energy, since a lightning strike creates waves of energy that travel from one side of the Earth to the other, acting in turn like a huge coil that can be set and maintained in resonance.

The ionosphere is also highly conductive and can therefore be exploited to transport electrical energy over long distances.

Our LBD laboratory studies into mixing radio wave frequencies within a volumetric space—surrounded by high-voltage sources, typically a Van de Graff generator, and dual or multiple Tesla coils—have yielded remarkable and reproducible outcomes, paving the way for the successful testing of our syntropic equipment.

Observed phenomena include the levitation of heavy payloads, the simultaneous fusion of disparate materials like metal and wood, and the anomalous heating and melting of metals without scorching adjacent surfaces. Furthermore, we have documented the spontaneous fracturing of metals exhibiting a lateral flow pattern, alongside both temporary and permanent alterations to the crystalline morphology and physical characteristics of metallic substances.